| Abstract: | We have investigated the hydrogeology of the Hualapai Valley, Detrital Valley, and Sacramento Valley basins of Mohave County in northwestern Arizona to develop a better understanding of groundwater storage within the basin fill aquifers. In our investigation we used geologic maps, well-log data, and geophysical surveys to delineate the sedimentary textures and lithology of the basin fill. We used gravity data to construct a basin geometry model that defines smaller subbasins within the larger basins, and airborne transient-electromagnetic modeled results along with well-log lithology data to infer the subsurface distribution of basin fill within the subbasins. Hydrogeologic units (HGUs) are delineated within the subbasins on the basis of the inferred lithology of saturated basin fill. We used the extent and size of HGUs to estimate groundwater storage to depths of 400 meters (m) below land surface (bls). The basin geometry model for the Hualapai Valley basin consists of three subbasins: the Kingman, Hualapai, and southern Gregg subbasins. In the Kingman subbasin, which is estimated to be 1,200 m deep, saturated basin fill consists of a mixture of fine- to coarse-grained sedimentary deposits. The Hualapai subbasin, which is the largest of the subbasins, contains a thick halite body from about 400 m to about 4,300 m bls. Saturated basin fill overlying the salt body consists predominately of fine-grained older playa deposits. In the southern Gregg subbasin, which is estimated to be 1,400 m deep, saturated basin fill is interpreted to consist primarily of fine- to coarse-grained sedimentary deposits. Groundwater storage to 400 m bls in the Hualapai Valley basin is estimated to be 14.1 cubic kilometers (km3). The basin geometry model for the Detrital Valley basin consists of three subbasins: northern Detrital, central Detrital, and southern Detrital subbasins. The northern and central Detrital subbasins are characterized by a predominance of playa evaporite and fine-grained clastic deposits; evaporite deposits in the northern Detrital subbasin include halite. The northern Detrital subbasin is estimated to be 600 m deep and the middle Detrital subbasin is estimated to be 700 m deep. The southern Detrital subbasin, which is estimated to be 1,500 m deep, is characterized by a mixture of fine- to coarse-grained basin fill deposits. Groundwater storage to 400 m bls in the Detrital Valley basin is estimated to be 9.8 km3. The basin geometry model for the Sacramento Valley basin consists of three subbasins: the Chloride, Golden Valley, and Dutch Flat subbasins. The Chloride subbasin, which is estimated to be 900 m deep, is characterized by fine- to coarse-grained basin fill deposits. In the Golden Valley subbasin, which is elongated north-south, and is estimated to be 1,300 m deep, basin fill includes fine-grained sedimentary deposits overlain by coarse-grained sedimentary deposits in much of the subbasin. The Dutch Flat subbasin is estimated to be 2,600 m deep, and well-log lithologic data suggest that the basin fill consists of interlayers of gravel, sand, and clay. Groundwater storage to 400 m bls in the Sacramento Valley basin is estimated to be 35.1 km3. |
| Genre: | USGS Numbered Series |
| ProdID: | 70043831 |
| Citation Author: | Truini, Margot ; Beard, L. Sue; Kennedy, Jeffrey ; Anning, Dave W. |
| Citation Contributing Office: | Arizona Water Science Center |
| Citation Datum: | |
| Citation Day: | |
| Citation Edition: | |
| Citation Editor: | |
| Citation End Page: | 47 |
| Citation Issue: | |
| Citation Keywords: | |
| Citation Language: | English |
| Citation Larger Work Title: | |
| Citation LatN: | 37.0 |
| Citation LatS: | 31.33 |
| Citation LonE: | -109.0 |
| Citation LonW: | -114.82 |
| Citation Month: | |
| Citation No Pagination: | |
| Citation Number Of Pages: | 56 |
| Citation Online Only Flag: | Y |
| Citation Phsyical Description: | vi, 47 p. |
| Citation Projection: | |
| Citation Public Comments: | Prepared in cooperation with the Arizona Department of Water Resources and Mohave County, Arizona |
| Citation Publisher: | U.S. Geological Survey |
| Citation Series: | Scientific Investigations Report |
| Citation Series Code: | SIR |
| Citation Series Number: | 2012-5275 |
| Citation Search Results Text: | Hydrogeologic framework and estimates of groundwater storage for the Hualapai Valley, Detrital Valley, and Sacramento Valley basins, Mohave County, Arizona; 2013; SIR; 2012-5275; Truini, Margot ; Beard, L. Sue; Kennedy, Jeffrey ; Anning, Dave W. |
| Citation Start Page: | i |
| Citation Volume: | |
| Citation Year: | 2013 |
| Type: | citation/reference |
| Text: | Hydrogeologic framework and estimates of groundwater storage for the Hualapai Valley, Detrital Valley, and Sacramento Valley basins, Mohave County, Arizona; 2013; SIR; 2012-5275; Truini, Margot ; Beard, L. Sue; Kennedy, Jeffrey ; Anning, Dave W. |
| URL (INDEX PAGE): | http://pubs.usgs.gov/sir/2012/5275/ |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/sir_2012_5275.gif |
| URL (DOCUMENT): | http://pubs.usgs.gov/sir/2012/5275/sir2012-5275.pdf |
| Date Other: | Wed, 20 Feb 2013 00:00 -0600 |
| Publisher: | U.S. Geological Survey |